(99) 
occurs in the New Jersey Raritan (localities not given); on 
Staten Island; and in the Atane and Patoot beds of Green- 
land. The genus was founded by Saporta & Marion* and 
embraces several European species of which Dewalguea in- 
signis reappears in both the Atane and Patoot beds of Green- 
land, and on Staten Island; while D. Haldem/ana reappears 
in the Patoot beds, in Utah, and on Staten Island. The 
Dakota group furnishes two additional species. 
PopozaAMITES MARGINATUS Heer. Fi. 46. f. 1-3. 
Podozamites marginatiis Heer, Fl. Foss. Arct. 67: 43. pi. 
16. f. 0. 
Similar remains are common in the Raritan (three species). 
Hollick (Bull. Torrey Club, 21: 62. A/. 180. f. 4) records a 
fragment from Glen Cove, Long Island, and also from Chap- 
paquidick Island, Mass. (Bull. N. Y. Bot. Gard. 2: 4o1. pi. 
41. f. 8, 9. 1902). 
The genus was founded by Fr. Braun, in Minster, Beitr. 
Petrefacten-Kunde (Heft. 6. 28. 1843) and is chiefly Upper 
Triassic (Rhetic) and Jurassic, becoming decadent in the 
Cretaceous. The latter has yielded, however, seventeen 
species on this continent (including Greenland), nine of which 
existed as late as the mid-Cretaceous, all described from 
rather fragmentary and somewhat doubtful leaf-remains. 
Our specimens would appear to be fragments of Podozam- 
ates marginatus? Heer, which occurs at Woodbridge in the 
Raritan clays (Fl. Amboy Clays, 44. pl. 13. fi 5. 6); 
originally described by Heer from Atane, Greenland. 
Phragmites (?) Cliffwoodensis sp. nov. Fl. 46. f. 5. 
A terminal, sharply pointed fragment of a monocotyle- 
donous leaf, 12 cm. long and 5.5 mm. broad, finely parallel- 
veined. 
The remains of Phragmites usually consists of leaf frag- 
ments or rhizomes, all of rather doubtful affinity, although a 
single palet of P. Oenzngensis A. Br. is described by Heer 
from Greenland. 
* Mem. Cour. & Sav. Etrangers Acad. Belg. 37: 55. 1873. 
